Evidence for archaeal methanogenesis within in situ veins at the onshore peridotite-hosted Chimaera seeps, Turkey

Jennifer Zwicker, Daniel Birgel, Wolfgang Bach, Sylvain Richoz, Susanne Gier, Daniel Smrzka, Christa Schleper, Simon Karl-Maria Rasso Rittmann, Bernhard Grasemann, Erdal Kosun, Jörn Peckmann

Serpentinite-hosted ecosystems have attracted the interest of the scientific community, as they are considered to be likely environments where life first evolved on Earth. Serpentinization reactions produce strongly reducing and highly alkaline fluids that are typified by high concentrations of molecular hydrogen and methane, which can be used as an energy source by chemotrophic microbial communities. Moreover, carbonate formation is a common late-stage alteration process that is induced by the serpentinization of peridotite at the seafloor and on land. It is well established that low-temperature serpentinization at slow-spreading mid-ocean ridges provides an ideal environment for rich microbial communities, including anaerobic archaea and bacteria. Recent studies of lipid biomarkers and their isotopic compositions have suggested that some Euryarchaeota are able to perform methanogenesis and methanotrophy, depending on the prevailing environmental conditions. However, no evidence for archaeal methanogenesis or methanotrophy has yet been reported for similar environments on land. This study is the first to present lipid biomarker evidence for archaeal methanogenesis at the terrestrial, peridotite-hosted Chimaera seep in Turkey. The analyzed Chimaera rock samples are serpentinites that are cross-cut by veins composed of brucite and hydromagnesite. Pentamethylicosane and squalane with delta13C values of +10‰ and +14‰, respectively, were identified within the brucite-carbonate veins. Furthermore, archaeol, sn2-hydroxyarchaeol, squalane and squalenes were found. Archaeol and sn2-hydroxyarchaeol also show high compound-specific delta13C values of up to +7‰. These isotope signals combined with the absence of crocetane – a biomarker for methanotrophic archaea – reveals that the microbial communities at the Chimaera Seep performed methanogenesis rather than methanotrophy. Our results suggest that biological methane production may play a role during terrestrial low-temperature serpentinization than previously recognized.

Institut für Geologie
Externe Organisation(en)
Universität Bremen, Karl-Franzens-Universität Graz, Musée cantonal de Géologie Lausanne, Akdeniz University, Universität Hamburg
ÖFOS 2012
105105 Geochemie, 105120 Petrologie, 105128 Geomikrobiologie
Sustainable Development Goals
SDG 15 – Leben an Land
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